Andes mountains

• Andes mountains

59:5.18Through­out this epoch the moun­tains of North and South Amer­ica were ac­tive, both the An­des and the south­ern an­ces­tral Rocky Moun­tains ris­ing. The great At­lantic and Pa­cific high coastal re­gions be­gan to sink, even­tu­ally be­com­ing so eroded and sub­merged that the coast lines of both oceans with­drew to ap­prox­i­mately their pres­ent po­si­tions. The de­posits of this in­un­da­tion av­er­age about one thou­sand feet in thick­ness.

• Andes mountains

60:2.6The same po­lar sea that ex­tended so far down over North Amer­ica like­wise cov­ered all of South Amer­ica ex­cept the soon ap­pear­ing An­des Moun­tains. Most of China and Rus­sia was in­un­dated, but the wa­ter in­va­sion was great­est in Eu­rope. It was dur­ing this sub­mer­gence that the beau­ti­ful litho­graphic stone of south­ern Ger­many was laid down, those strata in which fos­sils, such as the most del­i­cate wings of olden in­sects, are pre­served as of but yes­ter­day.

• Andes mountains

60:3.4100,000,000 years ago the North Amer­i­can con­ti­nent and a part of Eu­rope were well above wa­ter. The warp­ing of the Amer­i­can con­ti­nents con­tin­ued, re­sult­ing in the meta­mor­phos­ing of the South Amer­i­can An­des and in the grad­ual el­e­va­tion of the west­ern plains of North Amer­ica. Most of Mex­ico sank be­neath the sea, and the south­ern At­lantic en­croached on the east­ern coast of South Amer­ica, even­tu­ally reach­ing the pres­ent shore line. The At­lantic and In­dian Oceans were then about as they are to­day.